Electrical resistance of single-crystal magnetite (Fe3O4) under quasi-hydrostatic pressures up to 100GPa

被引:15
|
作者
Muramatsu, Takaki [1 ]
Gasparov, Lev V. [2 ]
Berger, Helmuth [3 ]
Hemley, Russell J. [1 ,4 ]
Struzhkin, Viktor V. [1 ]
机构
[1] Carnegie Inst Sci, Geophys Lab, Washington, DC 20015 USA
[2] Univ N Florida, Dept Phys, Jacksonville, FL 32224 USA
[3] Ecole Polytech Fed Lausanne, Lausanne, Switzerland
[4] Lawrence Livermore Natl Lab, Livermore, CA 94550 USA
基金
美国国家科学基金会;
关键词
VERWEY TRANSITION; METALLIZATION; CONDUCTIVITY;
D O I
10.1063/1.4945388
中图分类号
O59 [应用物理学];
学科分类号
摘要
The pressure dependence of electrical resistance of single-crystal magnetite (Fe3O4) was measured under quasi-hydrostatic conditions to 100 GPa using low-temperature, megabar diamond-anvil cell techniques in order to gain insight into the anomalous behavior of this material that has been reported over the years in different high-pressure experiments. The measurements under nearly hydrostatic pressure conditions allowed us to detect the clear Verwey transition and the high-pressure structural phase. The appearance of a metallic ground state after the suppression of the Verwey transition around 20 GPa and the concomitant enhancement of the electrical resistance caused by the structural transformation to the high-pressure phase form reentrant semiconducting-metallic-semiconducting behavior, although the appearance of the metallic phase is highly sensitive to stress conditions and details of the measurement technique. (C) 2016 AIP Publishing LLC.
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页数:6
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